Articles | Volume 34, issue 5
https://doi.org/10.5194/ejm-34-507-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/ejm-34-507-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Studies on the local structure of the F ∕ OH site in topaz by magic angle spinning nuclear magnetic resonance and Raman spectroscopy
Institut für Geologische Wissenschaften, Freie Universität
Berlin, Malteserstr. 74–100, 12249 Berlin, Germany
Gudrun Scholz
Institut für Chemie, Humboldt-Universität zu Berlin,
Brook-Taylor Str. 2, 12489 Berlin, Germany
Nader de Sousa Amadeu
Abteilung
Materialchemie, Bundesanstalt für Materialforschung und -prüfung, Richard-Willstätter-Str. 11, 124489 Berlin, Germany
Jingjing Shao
Institut für Chemie und Biochemie, Freie Universität Berlin,
Arnimallee 22, 14195 Berlin, Germany
Dina Schultze
Museum für Naturkunde, Invalidenstraße 43, 10115 Berlin,
Germany
Jeremy Fuller
Topaz Mountain Minerals – Utah Mineral Mining Inc., 84094 Sandy,
Utah, USA
Beate Paulus
Institut für Chemie und Biochemie, Freie Universität Berlin,
Arnimallee 22, 14195 Berlin, Germany
Franziska Emmerling
Abteilung
Materialchemie, Bundesanstalt für Materialforschung und -prüfung, Richard-Willstätter-Str. 11, 124489 Berlin, Germany
Thomas Braun
Institut für Chemie, Humboldt-Universität zu Berlin,
Brook-Taylor Str. 2, 12489 Berlin, Germany
Timm John
Institut für Geologische Wissenschaften, Freie Universität
Berlin, Malteserstr. 74–100, 12249 Berlin, Germany
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Metamorphic rocks contain information about their original rocks and thus provide insight into the earlier stages of a region of interest. Here, we used the whole-rock chemical composition and stable boron isotopes of a suite of rocks from the Alps (Italy–Austria), which were deposited in a restricted intramontane basin before the Alpine orogeny. It is possible to reconstruct the depositional conditions for these sediments, which are now common metamorphic rocks such as schists and gneisses.
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Tungsten (W) concentrations in fluids in equilibrium with crystalline tungsten oxide are used to improve constraints of thermodynamic parameters for W solubility. W species in the hydrothermal fluids are further characterized by X-ray spectroscopy. Improved thermodynamic properties for a set of W fluid species are provided that cover a wide range of fluid compositions, necessary for understanding and describing the complex processes of W enrichment and mineralization in hydrothermal systems.
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Metamorphic rocks contain information about their original rocks and thus provide insight into the earlier stages of a region of interest. Here, we used the whole-rock chemical composition and stable boron isotopes of a suite of rocks from the Alps (Italy–Austria), which were deposited in a restricted intramontane basin before the Alpine orogeny. It is possible to reconstruct the depositional conditions for these sediments, which are now common metamorphic rocks such as schists and gneisses.
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The amorphous phase of the natural mineral olivine was synthesized to investigate its mechanical properties. Tensile tests with in situ optical microscopy revealed brittle behaviour of amorphous olivine. Using digital image correlation, we estimated the intrinsic strength of amorphous olivine to be about 1.8 GPa. The measured intrinsic strength of amorphous olivine should help to better identify the “weak link” that initiates or promotes macroscopic material failure.
Catherine Leyx, Peter Schmid-Beurmann, Fabrice Brunet, Christian Chopin, and Christian Lathe
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We performed experimental measurements of elastic parameters of fayalite. The idea is to better define the effect of olivine Fe content on these parameters and test how sensitive these are when adjusting mineralogical models to seismic data. The trend of the olivine shear modulus with Fe content is well defined, but that of the bulk modulus remains less constrained, and more experiments on olivines with different Fe compositions are needed.
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Water plays an important role in the physical properties (i.e., diffusivity, electrical conductivity, thermal conductivity, sound velocity, and rheology) of olivine, wadsleyite, and ringwoodite. Remarkably, there are numerous discrepancies and debates between experimental and theoretical studies. Here we provide a comprehensive review of the recent advances in the influence of water on the physical properties of olivine, wadsleyite, and ringwoodite, together with their applications.
Simon Breuer and Frank R. Schilling
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The knowledge of physical properties of quartz as an abundant rock-forming mineral in the Earth’s crust allows for a better understanding of its dynamic processes. The thermal transport properties of single-crystal quartz are studied between –120 °C and 800 °C using a laser flash method. First, low-temperature data as well as the role of the low-to-high quartz phase transition (e.g. a transition-related non-ballistic radiative transfer) and size effects on thermal diffusivity are discussed.
Reinhard X. Fischer, Manfred Burianek, and Robert D. Shannon
Eur. J. Mineral., 32, 27–40, https://doi.org/10.5194/ejm-32-27-2020, https://doi.org/10.5194/ejm-32-27-2020, 2020
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It is shown here that the H2O content of hydrous minerals can be determined from their mean refractive indices with high accuracy. This is especially important when only small single crystals are available. Such small crystals are generally not suitable for thermal analyses or for other reliable methods of measuring the amount of H2O. The results are compared with the observed H2O content evaluating 157 zeolite-type compounds and 770 non-zeolitic hydrous compounds, showing good agreement.
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Short summary
We investigated the effect that fluoride and protons have on each other as structural neighbors in the mineral topaz. This was done using spectroscopic methods, which measure the interaction of electromagnetic radiation with matter. The forces between atoms distort the spectroscopic signals, and this distortion can thus be used to understand the corresponding forces and their effect on the physical properties of the mineral.
We investigated the effect that fluoride and protons have on each other as structural neighbors...